Ferroskutterudite is an iron-rich member of the skutterudite group, characterized by its metallic silver-white color and cubic habit. Collectors typically find this rare arsenide mineral in cobalt-silver hydrothermal vein deposits alongside other arsenic-bearing minerals.
Is this ferroskutterudite?
4-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch ferroskutterudite with a known reference. Ferroskutterudite sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: tin white.
- 4Look at form & habitCrystal system: cubic. Typical habit: granular.
Often confused with
Ferroskutterudite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ferroskutterudite
Minerals reported to co-occur with ferroskutterudite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeAs₃
- Mohs hardness
- 6-6.5
- Density
- 6.7-6.9 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular
- Cleavage
- Perfect, probably on {02̄1}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermal dolomite-calcite veins and apophyllite-anhydrite-carbonate veins in a magmatic hydrothermal Co-Ni antimonide-arsenide deposit
Where rockhounds find ferroskutterudite
Classic worldwide localities
- Noril’sk ore field, Russia
Field-hunting tip
Where it forms: In hydrothermal dolomite-calcite veins and apophyllite-anhydrite-carbonate veins in a magmatic hydrothermal Co-Ni antimonide-arsenide deposit. If you start seeing wurtzite, sphalerite, galena in float, you are in the right ground. Typical habit: granular. Train your eye for that shape before scanning the outcrop.









